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NUMBER 89 113<br />

Dunedin<br />

FAR NORTH DUNES<br />

FIGURE 1.—Map of New Zealand showing the study areas on South Island, the four main cities (Auckland, Wellington,<br />

Christchuch, and Dunedin), major geographic features, and degrees of south latitude (numbered bars).<br />

Waitomo Caves and the Far North dunes are areas with important fossil deposits.<br />

vegetation was characterized by its mosaic nature and differed<br />

markedly from the closed-canopy forests of western regions.<br />

The faunas are from sites with diverse taphonomic histories:<br />

10 sites are Laughing Owl deposits, five are swamps, one is a<br />

cave pitfall, two are archaeological, and several are rockshelters<br />

(Worthy and Holdaway, 1996). Most faunas are of Holocene<br />

age, but one is late glacial (10,000-12,000 years old).<br />

The oldest is from Otiran deposits (>24,000-< 100,000 years<br />

old) in alluvial beds in the Waipara Valley.<br />

300km<br />

SOUTH CANTERBURY.—The South Canterbury study area is<br />

at an altitude of 200-400 m and is located between Fairlie,<br />

Raincliff, and Bluecliffs Station (25 km southwest of Timaru).<br />

The climate is very similar to that of the Waikari study area,<br />

and the late Holocene vegetation is assumed also to have been<br />

very similar.<br />

The 59 fossil sites include 27 Laughing Owl deposits, two<br />

falcon deposits, two swamps, and 28 cave pitfall or rockshelter<br />

deposits (Worthy, 1997). The deposits are up to 38,000 years<br />

old, although most are of late-Holocene age.

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